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| 1 | Burial Dissolution of Ordovician Granule Limestone in the Tahe Oilfield of the Tarim Basin,NW China,and Its Geological Significance显示文摘摘要:与岩石学上的全面研究,一些奥陶纪小粒石灰石的地质学和地球化学在 Tarim 盆的 Tahe 油矿取样,埋葬溶解的二个阶段作为在里面来源溶解被提出并且基于宏小宇宙的岩石学和地球化学特征采购溶解。在二个阶段的主要差别在起源和酸液体的动人的通行证。Geochemical 证据显示埋葬溶解液体可能是与有机物成熟和烃联系的器官的酸, CO2 和 H2S 的成分分解,和在里面来源液体自己在小粒石灰石来自有机物,但是 out-source 远主要从另外的陶土的碳酸盐岩石。那么,形成一座埋葬溶解水库源于在里面来源和 out-source 溶解。小粒石灰石第一在 situ 在在里面来源溶解下面形成了独立针孔,并且以后承受了更宽的溶解与采购沿着不顺从,缝接,差错和伙伴裂缝移动的液体。第二个阶段是更重要的,并且在阶层的矿物质作文和液体的热传送对流处于良好的竟技状态有利水库也是重要的。 | LIU Chunyan LIN Changsong WANG Yi WU Maobing | 2008 | Acta Geologica Sinica(English Edition)2008，82，3： | 8 |
| 2 | The hydrothermal karstification and its effect on Ordovician carbonate reservoir in Tazhong uplift of Tarim Basin, Northwest China显示文摘With a detailed study on petrology, mineralogy and geochemistry of some important Ordovician carbonate well core samples in Tazhong uplift of Tarim Basin, the distinguishing symbols of hydrothermal karstification are first put forward as the phenomena of rock hot depigmentation, hot cataclasm and the appearance of typical hydrothermal minerals such as fluorite, barite, pyrite, quartz and sphalerite. The main homogenization temperatures of primary fluid inclusions in fluorite are from 260 to 310℃, indicating the temperature of hydrothermal fluid. The fluid affected the dissolved rocks and showed typical geochemistry features with low contents of Na and Mg, and high contents of Fe, Mn and Si. The ratio of 3He/4He is 0.02Ra, indicating the fluid from the typical continental crust. The hydrothermal fluid karstification pattern may be described as follows: the hot fluid is from the Permian magma, containing dissolving ingredients of CO2 and H2S, and shifts along fault, ruptures and unconformity, and dissolves the surrounding carbonates while it flows. The mechanism of hydrothermal karstification is that the mixture of two or more fluids, which have different ion intensity and pH values, becomes a new unsaturated fluid to carbonates. The hydrothermal karstification is an important process to form hypo-dissolved pinholes in Ordovician carbonates of Tazhong uplift of Tarim Basin, and the forming of hydrothermal minerals also has favorable influence on carbonate reservoirs. | WU MaoBing WANG Yi ZHENG MengLin ZHANG WeiBiao LIU ChunYan | 2007 | Science China Earth Sciences2007，50，z2： | 7 |
| 3 | Single-zircon dating of Precambrian strata in the west sector of the northern Qilian Mountains and its geological significance显示文摘Single_zircon evaporation method was employed in the present study to determine the age of the iron_bearing rock series in Precambrian strata in the western sector of the northern Qilian Mountains. Three zircon ages from the diabase of the Aoyougou ophiolite previously put into Upper Lithologic Formation of the Zhulongguan Group are (1 840±2), (1 783±2) and (1 784±2) Ma respectively, whereas the zircon ages from the welded breccias in the Zhulongguan Group are (733±7), (738±4) and (604±6) Ma respectively. These results show that they should belong to the bottom of the middle Proterozoic and the upper part of upper Proterozoic respectively. | Jingwen Mao Zhaochong Zhang Jianmin Yang Biao Song Maobing Wu Guochao Zuo | 1998 | Chinese Science Bulletin1998，43，15： | 5 |
| 4 | Kremen proteins are Dickkopf receptors that regulate Wnt/beta-eatenin signaling 显示文摘 | MAOB WU W DAVIDSON G | 2002 | Nature2002，417，6889： | 1 |
| 5 | LDL-receptor-related protein 6 is a receptor for Dickkopf proteins显示文摘 | MaoB Wu W Li Y | 2001 | Nature2001，411，： | 1 |
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